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,{"id":3964,"text":"cir480 - 1963 - Preparation of water samples for carbon-14 dating","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"cir480","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"480","title":"Preparation of water samples for carbon-14 dating","docAbstract":"For most natural water, a large sample is required to provide the 3 grams of carbon needed for a carbon-14 determination. A field procedure for isolating total dissolved-carbonate species is described. Carbon dioxide gas is evolved by adding sulfuric acid to the water sample; the gas is then collected in a sodium hydroxide trap by recycling in a closed system. The trap is then transported to the dating laboratory where the carbon-14 is counted.","language":"ENGLISH","publisher":"United States Geological Survey,","doi":"10.3133/cir480","usgsCitation":"Feltz, H., and Hanshaw, B.B., 1963, Preparation of water samples for carbon-14 dating: U.S. Geological Survey Circular 480, iii, 3 p. :ill. ;27 cm., https://doi.org/10.3133/cir480.","productDescription":"iii, 3 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":123205,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1963/0480/report-thumb.jpg"},{"id":31050,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1963/0480/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db658935","contributors":{"authors":[{"text":"Feltz, H.R.","contributorId":49341,"corporation":false,"usgs":true,"family":"Feltz","given":"H.R.","email":"","affiliations":[],"preferred":false,"id":147909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanshaw, Bruce B.","contributorId":47350,"corporation":false,"usgs":true,"family":"Hanshaw","given":"Bruce","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":147908,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4120,"text":"cir476 - 1963 - Principal lakes of the United States","interactions":[],"lastModifiedDate":"2018-02-14T16:18:45","indexId":"cir476","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"476","title":"Principal lakes of the United States","docAbstract":"<p>The United States has about 250 fresh-water lakes that are known to have surface areas of 10 square miles or more. Nearly 100 of these are in Alaska, and 100 in Minnesota, Wisconsin, Michigan, New York,, and Maine.</p>\n<p>Thirty-four fresh-water lakes, exclusive of the Great Lakes, are known to have maximum depths of 250 feet or more. Twenty of these are in Alaska, and Alaska undoubtedly has more lakes of that depth which have not been sounded.</p>\n<p>The amount of water stored in natural lakes even exclusive of the Great Lakes is much greater than the amount stored in artificial reservoirs. With the exception of the Great Lakes, however, the economic value of natural lakes is surpassed by that of artificial reservoirs. Natural lakes are best known for the recreational advantages they afford.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir476","usgsCitation":"Bue, C.D., 1963, Principal lakes of the United States: U.S. Geological Survey Circular 476, iii, 22 p., https://doi.org/10.3133/cir476.","productDescription":"iii, 22 p.","numberOfPages":"26","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science 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,{"id":32743,"text":"pp379 - 1963 - Surficial geology and soils of the Elmira-Williamsport region, New York and Pennsylvania, with a section on forest regions and great soil groups","interactions":[],"lastModifiedDate":"2022-03-29T21:42:36.762876","indexId":"pp379","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"379","title":"Surficial geology and soils of the Elmira-Williamsport region, New York and Pennsylvania, with a section on forest regions and great soil groups","docAbstract":"<p>The Elmira-Williamsport region, lying south of the Finger Lakes in central New York and northern Pennsylvania, is part of the Appalachian Plateaus physiographic province. A small segment of the Valley and Ridge province is included near the south border. In 1953 and 1954, the authors, a geologist and a soil scientist, made a reconnaissance of about 5,000 square miles extending southward from the Finger Lakes, N.Y., to Williamsport, Pa., and eastward from Wellsboro, Pa., to Towanda, Pa. Glacial drift of Wisconsin age, covering the central and most of the northern parts of the region, belongs to the Olean substage of MacClintock and Apfel. This drift is thin and patchy, is composed of the relatively soft sandstones, siltstone, shales, and conglomerates of the plateaus, commonly has a low calcium carbonate content, and is deeply leached. Mantling its surface are extensive rubbly colluvial deposits. No conspicuous terminal moraine marks the relatively straight border of Olean drift. The Valley Heads moraine of Fairchild near the south ends of the Finger Lakes is composed of relatively thick drift containing a considerable amount of somewhat resistant sedimentary and crystalline rocks. Commonly this drift has a relatively high carbonate content and is leached to only shallow depths. The Valley Heads drift is younger than Olean, but its precise age is undetermined. The age of the Olean is perhaps between Sangamon and Farmdale, on the basis of, in part, a carbon-14 date from peat at Otto, N.Y. All differences in soil development on these two Wisconsin drifts are clearly related to the lithology of the parent material or the drainage, rather than to weathering differing in kind or in duration. The authors believe that the soils are relatively young, are in equilibrium with the present environment, and contain few, if any, features acquired during past weathering intervals. The effect of tree throw on soil profiles and the presence of soils on slopes clearly indicate that soils form rapidly. Sols Bruns Acides are the most extensive great soil group occurring throughout the region. Podzols and Gray-Brown Podzolic soils are also widespread, and on long, smooth slopes Low Humic-Gley soils are common. Organic soils are of small extent. South of the Wisconsin drift border, the surficial mantle consists chiefly of alluvial, colluvial, or residual deposits of Wisconsin or of Recent age, but there are many small isolated patches of older, strongly weathered materials of pre-Wisconsin age. Although such older materials are commonly overlain or mixed with less weathered mantle, the yellowish-red color, characteristic of the strongly weathered material, is generally not masked. Some of the older material is drift, presumed to be of Illionian age, that was probably strongly weathered to a considerable depth in Sangamon time and has been greatly eroded since the last interglacial period. No clear-cut exposure of Wisconsin drift resting on older drift or other strongly weathered mantle has been found. The old drift and the other strongly weathered materials apparently acquired their present red color in pre-Wisconsin time. Where exposed at the surface, such strongly weathered mantle is the parent material of modern Red-Yellow Podzolic soils. Sols Bruns Acides and Gray-Brown Podzolic soils, developed on slightly weathered parent materials, are found adjacent to these red soils. This suggests that these Red-Yellow Podzolic soils probably developed from strongly weathered parent materials. No buried soils were found nor were any soils recognized as relics from pre-Wisconsin time. Comparison of a map of the great soil groups with a map of the vegetation of the region, prepared by John C. Goodlett, does not reveal a close relation. Laboratory analyses of samples collected furnish data on textural, mineralogical, and chemical changes caused by weathering and soil formation. The results indicate that the amount of chemical weathering which the Wisconsin drift has undergone is slight. The Red-Yellow Podzolic soils on strongly weathered pre-Wisconsin drift have B2 horizons that have a finer texture than the A2 or C horizons. The parent materials of these soils seem to be strongly weathered because of the high chromas, reddish hues, friable condition of most rock fragments, relatively high kaolinite content, and presence of gibbsite in the clay fraction. Measurements at numerous localities show that the depth of leaching increases with decreasing carbonate content and is not a criterion of the age of the drift. Pebble counts of gravels also show that the depth of leaching of gravel is related to its limestone content. The location of the gravel deposits is probably due primarily to the presence of pebbles of resistant rock rather than to ice wastage involving abundant glacial melt water. The region is in the Susquehanna drainage basin except for its north fringe, which drains to Lake Ontario. Most of the region is a dissected plateau ranging in altitude from 700 to 2,500 feet and underlain by gently folded sedimentary rocks of Paleozoic age. Much of the region slopes moderately or steeply; the most extensive areas of gently sloping land are 011 the uplands. In the northern part are several straight and deep valleys the southern extension of the Finger Lakes basins separated by uplands with several low cuestas that face north. Similarly, some streams such as the Canisteo, Cohocton, and Chemung Rivers, and the part of the Susquehanna River that is in New York, trend at right angles to the Finger Lakes, flowing in valleys that parallel the regional strike of the bedrock. The Olean drift border is marked by a change from drift containing very few rounded or striated rock fragments to a mantle containing only angular rock fragments and traces of red, strongly weathered materials. A reconstruction of the surface of the ice sheet, at its maximum extent shows an inferred slope of its distal margin ranging from 100 to 500 feet per mile</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp379","usgsCitation":"Denny, C.S., Lyford, W.H., and Goodlett, J.C., 1963, Surficial geology and soils of the Elmira-Williamsport region, New York and Pennsylvania, with a section on forest regions and great soil groups: U.S. Geological Survey Professional Paper 379, Report: iv, 59 p.; 6 Plates: 41.94 × 24.00 inches or smaller, https://doi.org/10.3133/pp379.","productDescription":"Report: iv, 59 p.; 6 Plates: 41.94 × 24.00 inches or smaller","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":60663,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0379/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60662,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0379/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60661,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0379/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60660,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0379/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60659,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0379/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60664,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0379/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60665,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0379/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397823,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4377.htm"},{"id":121752,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0379/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"New York, Pennsylvania","otherGeospatial":"Elmira-Williamsport region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.5,\n              41.1667\n            ],\n            [\n              -76.25,\n              41.1667\n            ],\n            [\n              -76.25,\n              42.5\n            ],\n            [\n              -77.5,\n              42.5\n            ],\n            [\n              -77.5,\n              41.1667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688b83","contributors":{"authors":[{"text":"Denny, Charles Storrow","contributorId":86331,"corporation":false,"usgs":true,"family":"Denny","given":"Charles","email":"","middleInitial":"Storrow","affiliations":[],"preferred":false,"id":209081,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyford, Walter Henry","contributorId":43824,"corporation":false,"usgs":true,"family":"Lyford","given":"Walter","email":"","middleInitial":"Henry","affiliations":[],"preferred":false,"id":209080,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goodlett, J. C.","contributorId":98771,"corporation":false,"usgs":true,"family":"Goodlett","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":209082,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14075,"text":"ofr6345 - 1963 - Preliminary interpretation of an aeromagnetic survey in north-central Iowa","interactions":[],"lastModifiedDate":"2024-07-26T22:16:42.14486","indexId":"ofr6345","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"63-45","title":"Preliminary interpretation of an aeromagnetic survey in north-central Iowa","docAbstract":"<p>Publication of Lyons' gravity map of the United States in 1950 focused attention on a spectacular geophysical feature now generally referred to as the \"midcontinent gravity high.\" This feature, the largest gravity maximum in North America, was discovered and later detailed by geophysicists at the University of Wisconsin (Woollard, 1943, 1951) and Thiel (1956). Their work reveals an essentially continuous large positive gravity anomaly extending southwestward for 800 miles from Lake Superior to the Salina Basin in Kansas. The midcontinent gravity high reaches its maximum intensity in central Iowa where the Bouguer anomaly ranges from -100 to 60 milligals.</p><p>In September-October 1961, the U. S. Geological Survey made a 5,000 square mile aeromagnetic survey in north-central Iowa in cooperation with the Iowa Geological Survey. Objectives of the investigation were to prepare and interpret a detailed aeromagnetic contour map for part of the midcontinent gravity high in Iowa. Analysis of the magnetic data could be expected to yield estimates of local thickness of the Paleozoic-Mesozoic sedimentary section and provide a basis for informed speculation about the character, configuration, and distribution of the Precambrian rocks. Such information would have obvious scientific and possible economic value in an area covered by glacial till and for which little deep subsurface knowledge was available. Interpretation of the Indiana aeromagnetic survey (Henderson and Zietz, 1958) had previously demonstrated that aeromagnetic data from the central stable region of North America would provide a significant amount of geologic information.</p><p>The 5,000 square mile area surveyed in 1961 has been combined with a previously unpublished 600 square mile aeromagnetic survey made in 1953, centered on Manson, Pocahontas Co., Iowa. The combined area is shown as the patterned area in figure 1. The unpatterned area outlined on this same figure is the additional 10,000 square mile cooperative aeromagnetic survey made in the summer of 1962 to complete coverage of the midcontinent gravity high in Iowa.</p><p>The primary purpose of this report is to make the 1953 and 1961 aeromagnetic data available to the public in advance of more formal publication. Only salient magnetic features are discussed in this preliminary presentation and in a second report on results obtained during the 1962 flying. A more complete interpretation of the entire aeromagnetic survey will be prepared.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6345","collaboration":"Prepared in cooperation with the Iowa Geological Survey","usgsCitation":"Henderson, J.R., White, W., and Zietz, I., 1963, Preliminary interpretation of an aeromagnetic survey in north-central Iowa: U.S. Geological Survey Open-File Report 63-45, Report: 27 p.; 4 Figures: 36.03 x 23.90 inches or smaller, https://doi.org/10.3133/ofr6345.","productDescription":"Report: 27 p.; 4 Figures: 36.03 x 23.90 inches or smaller","costCenters":[],"links":[{"id":431530,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1963/0045/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431529,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1963/0045/figure-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431528,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1963/0045/figure-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431527,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1963/0045/figure-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431526,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1963/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":410197,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8045.htm","linkFileType":{"id":5,"text":"html"}},{"id":146687,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1963/0045/report-thumb.jpg"}],"country":"United States","state":"Iowa","otherGeospatial":"north-central Iowa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -95,\n              43.5\n            ],\n            [\n              -95,\n              42.333\n            ],\n            [\n              -92.5,\n              42.333\n            ],\n            [\n              -92.5,\n              43.5\n            ],\n            [\n              -95,\n              43.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69742d","contributors":{"authors":[{"text":"Henderson, John Richard","contributorId":52975,"corporation":false,"usgs":true,"family":"Henderson","given":"John","email":"","middleInitial":"Richard","affiliations":[],"preferred":false,"id":168890,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Walter S.","contributorId":34492,"corporation":false,"usgs":true,"family":"White","given":"Walter S.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":168889,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":168891,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":43368,"text":"ofr63111 - 1963 - Geology of the Narragansett Bay area, Rhode Island","interactions":[],"lastModifiedDate":"2012-02-02T00:10:09","indexId":"ofr63111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"63-111","title":"Geology of the Narragansett Bay area, Rhode Island","language":"ENGLISH","doi":"10.3133/ofr63111","usgsCitation":"Quinn, A.W., 1963, Geology of the Narragansett Bay area, Rhode Island: U.S. Geological Survey Open-File Report 63-111, 1 map., https://doi.org/10.3133/ofr63111.","productDescription":"1 map.","costCenters":[],"links":[{"id":162522,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81101,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0111/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e929","contributors":{"authors":[{"text":"Quinn, Alonzo W.","contributorId":19554,"corporation":false,"usgs":true,"family":"Quinn","given":"Alonzo","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":228101,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43709,"text":"ofr63110 - 1963 - Geologic maps and sections of part of the Philipsburg district, Granite County, Montana","interactions":[{"subject":{"id":43709,"text":"ofr63110 - 1963 - Geologic maps and sections of part of the Philipsburg district, Granite County, Montana","indexId":"ofr63110","publicationYear":"1963","noYear":false,"title":"Geologic maps and sections of part of the Philipsburg district, Granite County, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":35523,"text":"b1237 - 1967 - Geology and ore deposits of the Philipsburg district, Granite County, Montana","indexId":"b1237","publicationYear":"1967","noYear":false,"title":"Geology and ore deposits of the Philipsburg district, Granite County, Montana"},"id":1}],"supersededBy":{"id":35523,"text":"b1237 - 1967 - Geology and ore deposits of the Philipsburg district, Granite County, Montana","indexId":"b1237","publicationYear":"1967","noYear":false,"title":"Geology and ore deposits of the Philipsburg district, Granite County, Montana"},"lastModifiedDate":"2020-02-03T12:46:21","indexId":"ofr63110","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"63-110","title":"Geologic maps and sections of part of the Philipsburg district, Granite County, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr63110","usgsCitation":"Prinz, W.C., 1963, Geologic maps and sections of part of the Philipsburg district, Granite County, Montana: U.S. Geological Survey Open-File Report 63-110, 7 Plates: 31.90 x 41.13 inches or smaller, https://doi.org/10.3133/ofr63110.","productDescription":"7 Plates: 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Dakota\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bea2","contributors":{"authors":[{"text":"Dobrovolny, Ernest","contributorId":45288,"corporation":false,"usgs":true,"family":"Dobrovolny","given":"Ernest","affiliations":[],"preferred":false,"id":224546,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39034,"text":"pp344B - 1963 - Anorthosite and associated rocks in the Boehls Butte quadrangle and vicinity, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:10:36","indexId":"pp344B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"344","chapter":"B","title":"Anorthosite and associated rocks in the Boehls Butte quadrangle and vicinity, Idaho","language":"ENGLISH","doi":"10.3133/pp344B","usgsCitation":"Hietanen, A., 1963, Anorthosite and associated rocks in the Boehls Butte quadrangle and vicinity, Idaho: U.S. Geological Survey Professional Paper 344, p. B1-B78, https://doi.org/10.3133/pp344B.","productDescription":"p. B1-B78","costCenters":[],"links":[{"id":120270,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0344b/report-thumb.jpg"},{"id":66216,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0344b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66217,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0344b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b5da","contributors":{"authors":[{"text":"Hietanen, Anna","contributorId":43841,"corporation":false,"usgs":true,"family":"Hietanen","given":"Anna","affiliations":[],"preferred":false,"id":220832,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57724,"text":"ofr63147 - 1963 - Tests of crest-stage gage intakes","interactions":[],"lastModifiedDate":"2026-01-26T16:54:15.528383","indexId":"ofr63147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"63-147","title":"Tests of crest-stage gage intakes","docAbstract":"<p>Various types of c rest-stage gages have been used by the Geological Survey. Most installations consist of a vertically mounted metal pipe, a wooden rod, an intake device, and a small amount of granulated cork. These gages are placed where elevations of flood crests are desired. Water rising and then falling in the gage leaves a high-water mark of granulated cork on the wooden rod. The elevation of this mark can be determined at a date subsequent to the date of the crest.</p><p>It has been found that the high-water mark left on the rod may not represent the true elevation of the flood crest in the stream at the gage site. The difference between the true elevation of the crest at the gage and the recorded elevation will be designated drawdown if the recorded elevation is less than the true elevation, or pileup if the recorded elevation is greater than the true elevation. Tests of drawdown and pileup effects have been made in the past by Survey personnel and others. (See p. 8.) These investigations have sometimes brought forth conflicting results, probably due to the varied conditions under which the gages were tested.</p><p>The purpose of this investigation was (1) to determine the pileup and drawdown characteristics of the intakes now being used by the Survey and (2) to design a better intake if existing models were found unsuitable. It was further prescribed that any new design that might result should be easily fabricated from standard pipe fittings, and should be unaffected by pileup or drawdown in excess of 0.1 foot for velocities up to about 8 feet per second.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr63147","usgsCitation":"Carter, J.R., and Gamble, C.R., 1963, Tests of crest-stage gage intakes: U.S. Geological Survey Open-File Report 63-147, 10 p., https://doi.org/10.3133/ofr63147.","productDescription":"10 p.","numberOfPages":"10","costCenters":[],"links":[{"id":499023,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1963/0147/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184244,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1963/0147/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6845d0","contributors":{"authors":[{"text":"Carter, Jack R.","contributorId":71632,"corporation":false,"usgs":true,"family":"Carter","given":"Jack","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":257644,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gamble, Charles R.","contributorId":6822,"corporation":false,"usgs":true,"family":"Gamble","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":257643,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38960,"text":"pp417B - 1963 - Some relations between streamflow characteristics and the environment in the Delaware River region","interactions":[],"lastModifiedDate":"2022-09-16T21:44:23.016232","indexId":"pp417B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"417","chapter":"B","title":"Some relations between streamflow characteristics and the environment in the Delaware River region","docAbstract":"<p>Streamflow characteristics are determined by a large number of factors of the meteorological and terrestrial environments. Because of lack of quantitative data to describe some of the factors and complex interrelations among them, complete analysis of the relations between streamflow and the various environmental factors is impossible. However, certain simplifying assumptions and generalizations made possible a partial analysis for the Delaware River region. For relations involving average runoff or low-flow parameters, average annual precipitation was assumed to be the principal meteorological factor, and geology (a complex of many factors) was assumed to be the principal terrestrial influence, except for that of basin size which was largely eliminated by expression of discharge in terms of unit area. As a first approximation, physiographic units were used as a basis for classifying the geology. Relations between flow parameters and precipitation are fairly well defined for some physiographic units, but not for those in which the geology varies markedly or the areal variation in average precipitation is very small. These relations provide a basis for adjusting the flow parameters to reduce or eliminate the effects of areal variations in precipitation and increase their significance in studies of the effects of terrestrial characteristics. An investigation of the residual effect of basin size (the effect remaining when discharge is expressed in terms of unit area) on relations between flow parameters and average precipitation indicates that such effect is negligible, except for very large differences in area. Parameters that are derived from base-flow recession curves and are related to a common discharge per unit area have inherent advantages as indicators of effects of terrestrial characteristics of basins, because the.y are independent of areal variations in average annual precipitation. Winter base-flow parameters are also practically independent of the effects of evapotranspiration from ground water. However, in many parts of the region these advantages are reduced or nullified by the difficulties of defining base-flow recession curves, particularly winter curves, with sufficient accuracy. In the absence of suitable base-flow recession data and a suitable basis for adjusting parameters, the ratio of the discharge equaled or exceeded 90 percent of the time to the average discharge (Qtt/Qa), or a similar duration parameter, probably is the best indicator of the influence of terrestrial characteristics, although the ratio may vary somewhat with average precipitation. In a part of the region where geologic differences are large and areal variations in average precipitation are small, values of Qm/Qa for each major geologic unit were determined from streamflow records. From these values and the percentage of area represented by each unit, a ratio for each gaging station was computed. Comparison of these computed results with the observed results indicates that nearly all of the variation in the ratio is associated with variation in geology. The investigation indicates that the original assumptions are correct; average precipitation is the principal meteorological influence and geology is the principal terrestrial influence. Together these two factors account for a very large proportion of the variation in average runoff and low-flow characteristics.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp417B","usgsCitation":"Hely, A., and Olmsted, F.H., 1963, Some relations between streamflow characteristics and the environment in the Delaware River region: U.S. Geological Survey Professional Paper 417, 25 p., https://doi.org/10.3133/pp417B.","productDescription":"25 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":406893,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4409.htm","linkFileType":{"id":5,"text":"html"}},{"id":122039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0417b/report-thumb.jpg"},{"id":66021,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0417b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0417b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66022,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0417b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Delaware, New Jersey, Pennsylvania","otherGeospatial":"Delaware River region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.4083,\n              39.5833\n            ],\n            [\n              -74.4417,\n              39.5833\n            ],\n            [\n              -74.4417,\n              41\n            ],\n            [\n              -76.4083,\n              41\n            ],\n            [\n              -76.4083,\n              39.5833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e8e4b07f02db5e8cd4","contributors":{"authors":[{"text":"Hely, A. G.","contributorId":14401,"corporation":false,"usgs":true,"family":"Hely","given":"A. G.","affiliations":[],"preferred":false,"id":220728,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olmsted, F. H.","contributorId":24765,"corporation":false,"usgs":true,"family":"Olmsted","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":220729,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2205,"text":"wsp1669K - 1963 - Correlation of water-level fluctuations with climatic cycles in the Oklahoma Panhandle","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1669K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1669","chapter":"K","title":"Correlation of water-level fluctuations with climatic cycles in the Oklahoma Panhandle","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669K","usgsCitation":"Marine, I.W., 1963, Correlation of water-level fluctuations with climatic cycles in the Oklahoma Panhandle: U.S. Geological Survey Water Supply Paper 1669, iii, 10 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1669K.","productDescription":"iii, 10 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":138170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669k/report-thumb.jpg"},{"id":27874,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669k/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27875,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db68454c","contributors":{"authors":[{"text":"Marine, I. Wendell","contributorId":49339,"corporation":false,"usgs":true,"family":"Marine","given":"I.","email":"","middleInitial":"Wendell","affiliations":[],"preferred":false,"id":144824,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52345,"text":"ofr6390 - 1963 - Aquifer-test compilation for the Mojave Desert region, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:32","indexId":"ofr6390","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"63-90","title":"Aquifer-test compilation for the Mojave Desert region, California","language":"ENGLISH","doi":"10.3133/ofr6390","usgsCitation":"McClelland, E., 1963, Aquifer-test compilation for the Mojave Desert region, California: U.S. Geological Survey Open-File Report 63-90, 26 p., https://doi.org/10.3133/ofr6390.","productDescription":"26 p.","costCenters":[],"links":[{"id":178914,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1963/0090/report-thumb.jpg"},{"id":86827,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1963/0090/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679e9c","contributors":{"authors":[{"text":"McClelland, E.J.","contributorId":54280,"corporation":false,"usgs":true,"family":"McClelland","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":245191,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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